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SUMMARY:NOTE TIME! 1-2pm! Cryptic Neoproterozoic mountain building events 
 around the margin of Rodinia - Rob Strachan\, University of Portsmouth
DTSTART:20120221T130000Z
DTEND:20120221T140000Z
UID:TALK35695@talks.cam.ac.uk
CONTACT:John Maclennan
DESCRIPTION:New insights into the Neoproterozoic geology of the Shetland I
 slands\, northernmost Scotland\, reflect the operation of the supercontine
 nt cycle. Sedimentary sequences accumulated in this part of Laurentia at ~
 1.0 Ga as a result of the erosion of the Grenville belt\, the culminating 
 collision event that formed Rodinia. Their subsequent deformation and meta
 morphism is inferred to result from terrane accretion events along a perip
 heral or exterior orogen that developed along the Laurentian margin of Rod
 inia. 
LOCATION:Harker 1 seminar room\, Department of Earth Sciences
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